中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
The spatial variability of streambed vertical hydraulic conductivity in an intermittent river, northwestern China

文献类型:EI期刊论文

作者Yu Jingjie; Liu Changming; Zhu Juntao; Wang Ping
发表日期2013
关键词Rivers Groundwater Hydraulic conductivity
英文摘要Streambed vertical hydraulic conductivity (K) plays an important role in river water and groundwater interaction. The K at the ten transects (Ts1-Ts10) at the Donghe River (an intermittent river) in the Ejina Basin, northwestern China, was measured to investigate its spatial variation. Based on the sediment characteristics and vertical hydraulic conductivity of the riverbed, the entire riverbed of the Donghe River could be divided arbitrarily into two parts: an upper part (starting at Ts1 and ending at Ts9, without an obvious and continuous clogging layer) and a lower part (the remaining riverbed, with an obvious and continuous clogging layer). In the upper part, although the K varied with depth within the 0-30 cm layer, the variability with depth could be ignored in practice. The arithmetic mean K of the upper part ranged from 12 to 27.6 m/day, three orders of magnitude larger than that of the lower part (0.06 m/day). The change of K along the river cross section was significant, and larger values of K often occurred in the parts of the channels with greater water depth. However, there were no consistent patterns of the variability of K at transects across the river, which was influenced by the variation in streambed characteristics. The results could be useful for the estimation of groundwater recharge from river and groundwater resources evaluation in the Ejina Basin. 2012 Springer-Verlag.
出处Environmental Earth Sciences
69期:3页:873-883
收录类别EI
语种英语
源URL[http://ir.igsnrr.ac.cn/handle/311030/31333]  
专题地理科学与资源研究所_历年回溯文献
推荐引用方式
GB/T 7714
Yu Jingjie,Liu Changming,Zhu Juntao,et al. The spatial variability of streambed vertical hydraulic conductivity in an intermittent river, northwestern China. 2013.

入库方式: OAI收割

来源:地理科学与资源研究所

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